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Scientific Reports logoLink to Scientific Reports
. 2021 Mar 25;11:6833. doi: 10.1038/s41598-021-86339-3

Nucleation of Ga droplets self-assembly on GaAs(111)A substrates

Artur Tuktamyshev 1,3,, Alexey Fedorov 2,3, Sergio Bietti 1,3, Stefano Vichi 1,3, Riccardo Tambone 1,3, Shiro Tsukamoto 1,3, Stefano Sanguinetti 1,3
PMCID: PMC7994575  PMID: 33767304

Abstract

We investigated the nucleation of Ga droplets on singular GaAs(111)A substrates in the view of their use as the seeds for the self-assembled droplet epitaxial quantum dots. A small critical cluster size of 1–2 atoms characterizes the droplet nucleation. Low values of the Hopkins-Skellam index (as low as 0.35) demonstrate a high degree of a spatial order of the droplet ensemble. Around 350C the droplet size distribution becomes bimodal. We attribute this observation to the interplay between the local environment and the limitation to the adatom surface diffusion introduced by the Ehrlich–Schwöbel barrier at the terrace edges.

Subject terms: Materials science, Nanoscience and technology, Physics

Introduction

The unique properties of the self-assembled quantum dots (QDs), such as the discrete energy levels and a precise control of additional features, like entangled photon emission, by the QD shape and size, have a great potential in the optoelectronic device fabrication for the future quantum network applications14. For this reason, one of the main challenges in the QD self-assembly is the reproducibility of QDs in terms of shape and size.

Droplet epitaxy (DE) is well-established for the formation of III-V compound semiconductor nanostructures and allows to control the QD density and size in a wide range5,6. The size distribution of the self-assembled DE QDs is strictly determined by the original size distribution of the droplets7. As the droplet size distribution can be easily controlled, using DE technique, it is then possible to obtain a narrow QD size distribution, resulting in a small ensemble photoluminescence linewidth8.

The (111)-oriented surfaces show a C3v symmetry, which allows to self-assemble highly symmetric QDs. These are necessary to reduce the fine structure splitting of the exciton state for the generation of highly entangled photons911. The QD self-assembly on (111) surfaces is complex using the Stranski-Krastanov (SK) growth mode12 (only recently the self-assembly of SK QDs on the (111)A surface was demonstrated13,14 by taking profit of tensile strain). Nevertheless, DE allows the density and the size control of the self-assembled QDs on (111)A surfaces11,15. Recently, the studies of shape-controlled highly symmetric DE GaAs QDs grown on AlGaAs/GaAs(111)A11 for entangled photon pair generation10 have been published. An additional interest to (111)A face is related to the possibility to self-assemble DE QDs without the formation of the wetting layer under the QD layer, since GaAs(111)A surface is in Ga-rich conditions and the deposition of group III atoms on the surface leads to immediate nucleation of the liquid droplets.

The epitaxial growth on (111) surfaces is complicated because the surface morphology is affected by the growth conditions. Nevertheless, using low growth rate and high V/III flux ratio for the growth of GaAs and AlGaAs layers on GaAs(111)A, it is possible to suppress an amount of hillocks nucleated by the stacking faults16 to improve the crystalline quality of the epitaxial layers.

In this work, we investigated the Ga droplet self-assembly on singular GaAs(111)A substrates in order to gain fundamental understanding of the effects of the surface characteristics, in terms of a surface reconstruction and a morphology, on the island nucleation dynamics. The droplet density dependence on the temperature has been determined in the temperature range between 300 and 450C. This gave us access to the fundamental physical quantities which determine the droplet formation dynamics: (1) the critical nucleus size for the droplet formation17,18; (2) the adatom surface diffusivity and its dependence on the surface reconstruction. We have also investigated the effect of surface defects on the droplet size distribution in combination with the presence of the sizeable Ehrlich–Schwöbel barrier typical for the GaAs(111)A surface16.

Methods

The samples were grown, using a molecular beam epitaxy (MBE) system, on an undoped singular GaAs(111)A substrates. The substrate temperature was measured by the thermocouple situated between the substrate heater and the sample, and by the infrared pyrometer.

After an oxide desorption at 590C, a 50 nm GaAs buffer layer was deposited at the temperature of 520C with a deposition rate of 0.07 ML/s (here and below 1 ML is defined as 6.26×1014atoms/cm2, which is the site-number density of the unreconstructed GaAs(001) surface), in order to obtain a smooth surface16. The substrate temperature was then decreased to the droplet deposition temperature varying from 300 to 450C. During the droplet deposition the As cell valve was closed in order to deplete the growth chamber from the arsenic molecules. 2 ML of gallium were deposited at a rate of 0.01 ML/s. During the Ga deposition, the background pressure was below 3×10-9 torr. The supply of Ga without As4 enabled the appearance of the Ga liquid droplets on the buffer layer surface. Next, an As4 flux with a beam equivalent pressure (BEP) of 6.2×10-5 torr was supplied at the same temperature for 3 minutes, in order to crystallize Ga droplets into GaAs islands. The sample T2b was arsenized after 30 minutes of annealing of Ga droplets at 350C, in order to study the influence of the ripening processes on the island density and size.

As shown in Refs.1921, the density of DE QDs, when crystallized at the same temperature used for the deposition of the metal droplets, mirrors that of droplets, thus making possible to access the density dependence of Ga droplets on the deposition parameters through the measurement of the island density. The crystallized surface morphology is more stable on time and avoids the strong oxidation effects which would hinder the reproducibility of the atomic force microscope (AFM) measurements.

The ex-situ morphological characterization of the samples was performed by AFM in a tapping mode, using tips capable of a lateral resolution of about 2 nm.

The growth description of the samples is summarized in Table 1.

Table 1.

The substrate temperature during the Ga droplet nucleation and the subsequent arsenization of the samples, presented in this work as well as the GaAs island density of the samples.

Sample T,C N,cm-2 Comments
T1 300 (7.67±1.15)×1010
T2 350 (1.83±0.06)×1010
T2b 350 (1.85±0.09)×1010 Arsenization after 30 minutes annealing
T3 400 (2.27±0.05)×109
T4 450 (7.17±1.08)×108

Results and discussion

Figure 1 shows AFM images of the samples T1, T2, T3, and T4 with GaAs islands, grown at 300, 350, 400, and 450C, respectively. The GaAs islands grown at 300C show a hexagonal shape. With the increasing the crystallization temperature the shape of islands becomes triangular. This observation in agreement with previous reports and it is related to the crystallization kinetics of the islands11,15. As expected, with increasing the deposition temperature the island density decreases1922. This tendency satisfies the classical nucleation theory of Venables17,18, which describes a nucleation of Ga droplets as a thermally activated process. As a result, the density of droplets N is reproduced by the Arrhenius law:

Nexp(Ea/kBT), 1

where Ea is the nucleation activation energy, kB—the Boltzmann’s constant, and T is the Ga droplet deposition temperature.

Figure 1.

Figure 1

AFM topography images of GaAs islands grown on the GaAs(111)A substrate at (a) 300C (1×1μm2, sample T1); (b) 350C (1×1μm2, sample T2); (c) 400C (1×1μm2, sample T3); (d) 450C (1×1μm2, sample T4). The red circle highlights a kinked island.

It is worth to mention that some of DE GaAs islands, grown on a singular GaAs(111)A surface, are “kinked” (Ga droplets are spontaneously crystallized in a horizontal direction). One kinked dot is highlighted on Fig. 1d. The analogues of such islands are kinked nanowires (NWs) performed by the vapor-liquid–solid (VLS) growth on (111) surfaces2325. The growth in a horizontal direction and a subsequent formation of kinked NWs is induced by a twin-mediated mechanism, which can be suppressed/maintained by controlling the growth conditions24,25. This behavior of a spontaneous nucleation of kinked GaAs islands on singular GaAs(111)A surface is in agreement with the expected island formation during the crystallization (arsenization) process of Ga droplets under the VLS mechanism.

Using the Arrhenius plot of the density dependence on the deposition temperature, it is possible to calculate the activation energy Ea. Figure 2a shows the temperature density dependence of GaAs islands in the range of 300–450C. The temperature error bar in our measurements is associated with the accuracy of the substrate temperature determination by the thermocouple and equals roughly ±5C. The density calculation was carried out using the data of several AFM scans from different areas of the samples. The density ranges from 7×108cm-2 to 8×1010cm-2. The activation energy, calculated from the temperature dependence of the island density, is 1.13±0.13eV. This value is in between the ones, which we calculated for the Ga droplet nucleation on vicinal GaAs(111)A21. It is assumed that the the Ga droplet nucleation on singular GaAs(111)A is characterized by both types of diffusion (one- and two-dimensional).

Figure 2.

Figure 2

(a) The temperature density dependence of DE GaAs islands grown on GaAs(111)A substrate (red points). The green star indicates the island density of the sample T2b. The nucleation activation energy, Ea=1.13±0.13eV. (b) The temperature dependence of a mean size of Voronoi cells. The activation energy Ea, calculated from this method, equals 1.13±0.23 eV. The temperature error bar for both graphs is ±5C.

A drastic change in the slope of the Arrhenius plot at T >200C was observed previously for the temperature density dependence of DE GaAs19 and islands grown on GaAs(001) and Ga droplets on singular GaAs(111)A22. Such a phenomenon was attributed to the onset of the Ostwald ripening process (the growth of large clusters on the cost of smaller ones and hence a decrease of the total cluster density in a closed thermodynamic system26) with increasing the deposition temperature. The change in the density of DE InAs QDs on GaAs(001) grown by metal-organic chemical vapor deposition was also associated with the Ostwald ripening during the nucleation of In droplets27. In the present work we did not observe such a change of the Arrhenius slope. In order to check the presence of the Ostwald ripening, we prepared the sample T2b, for which the arsenization process was carried out after 30 minutes of an annealing process at the same temperature. The island density of the sample equals (1.85±0.09)×1010cm-2 (the green star on Fig. 2a). The value is only slightly higher than that observed in the sample T2 - (1.83±0.06)×1010cm-2, for which the annealing was not performed. This suggests that no Ostwald ripening occurs after the deposition of Ga droplets in our experiments.

Additionally, the characteristic parameters of the nucleation process such as the activation energy Ea and the size of stable cluster i (the number of atoms that are the part of the largest unstable cluster17,18) can be obtained from the capture zone distribution (CZD) approach21,28,29. The capture zone (CZ) is the area from which, on average, the adatom constituting the island are collected. The exact shape of the normalized distribution of CZs strictly depends on the processes at the basis of the nucleation process28. The CZs can be determined from the Voronoi approach, a particular case of a surface tessellation where, given a set of centers (in our case the droplets), the space is divided according to their “area of influence”. In fact, the Voronoi cell identifies the area of the surface that is closer to the cell center respect to any other in the ensemble. CZD analysis provides an information about the size of the critical cluster and reflects the dimensionality of the nucleation process and can be extended to any aggregation-limited process29. Using this approach, the critical cluster size can be directly obtained from AFM scans and compared to the value, estimated from the droplet density dependence on the flux rate.

Figure 2b shows the temperature dependence of a mean size of Voronoi cells for the samples T1, T2, T3, and T4. Naturally, the total number of Voronoi cells are related to the island density, so using this dependence, it is also possible to determine Ea. From the CZD approach Ea=1.13±0.23eV, which is in agreement with the value determined from the island density dependence.

In order to determine the critical cluster size i, we analyzed normalized (to the mean size of Voronoi cells) CZD from the Voronoi tessellation. The predicted analytical form of CZD coincides with generalized Wigner distribution (GWD), proposed for the nearest-neighbor spacing distribution21,28,29 (see Fig. 3):

Pβ(s)=aβsβexp(-bβs2), 2

where s is the capture zone (CZ) area divided by its average value, aβ and bβ are the constants that assure the normalization and the unit mean conditions, respectively.

Figure 3.

Figure 3

CZDs of the samples (a) T1, (b) T2, (c) T3, and (d) T4, fitted by the GWD.

The fitting parameter β depends on i and the dimensionality of the diffusion γ as21,29

β=γi+γ+i. 3

The parameter β and the critical cluster size i obtained with γ = 1 (taking into account a two-dimensional adatom diffusion21,29) are presented in Table 2. For T400C the critical cluster size for the Ga droplet nucleation on singular GaAs(111)A i = 1–2 atoms, which is in good agreement with the previous studies21,22. We observed an increase of the critical cluster size at 450C, which is compatible with the expected stable cluster decomposition due to the thermally activated atom detachment processes17,18.

Table 2.

The fitting parameter β and the critical cluster size i of the samples T1, T2, T3, and T4.

Sample β i=β-2
T1 (300C) 4.3±0.4 2.3±0.4
T2 (350C) 3.0±0.4 1.0±0.4
T3 (400C) 4.0±0.2 2.0±0.2
T4 (450C) 6.0±0.3 4.0±0.3

The diffusivity behavior of Ga adatoms can be monitored through the spatial neighbor distribution of islands21. In Fig. 4 we report the two-dimensional histogram of the island-island relative distance Ri-Rj, where Ri and Rj indicate the position of two different islands, for sample T1. The rest of the samples show similar distribution, but with lower statistics, since the island density is higher at lower deposition temperature. The histogram shows that there is, on average, an excluded area (the area without the neighboring islands, highlighted by black lines) around each island with an almost symmetrical, nearly hexagonal, shape with the vertices in the <21¯1¯> directions. The shape of the excluded zone suggests that <21¯1¯> directions are preferable for the Ga adatom diffusion on GaAs(111)A. This observation is in agreement with the Ga-vacancy (2×2) surface reconstruction of GaAs(111)A30,31. According to Ref.31, the diffusion activation energies Ed equal 1.06 and 1.14 eV for Ga adatom diffusion in the <21¯1¯> and <11¯0> directions, respectively, on the GaAs(111)A-(2×2) surface reconstruction. Thus, the diffusion length in the <21¯1¯> directions should be longer, which we observed from the excluded zone area.

Figure 4.

Figure 4

Island-island distance distribution histogram showing the spatial neighbor distribution of GaAs islands for the sample T1 (80×80 nm2). The bin value color code is indicated.

The last goal of this work is to study a size distribution of the grown islands. Figure 5 shows the GaAs island height distribution of the samples T1, T2, T3, and T4 fitted by the Gaussian line shapes. At the low deposition temperature of 300C the size distribution has a mean island height of about 2.7 nm with a standard deviation of 43% (Fig. 5a). Similar situation at the high temperature of 450C (Fig. 5d). The mean height for the sample T4 is about 15.3 nm with the standard deviation of 45%. And the most intriguing observation is the presence of a bimodal island size distribution at the intermediate temperatures (350-400C). The sample T2 (Fig. 5b) has two groups of islands with the mean heights of 4.1 and 8.7 nm. And the mean island heights for sample T3 (Fig. 5c) are 7.0 and 14.8 nm. For both cases the aspect ratio R (the height over the base) of bigger islands is approximately two times larger than the one of smaller islands.

Figure 5.

Figure 5

The GaAs island height distribution of samples (a) T1, (b) T2, (c) T3, and (d) T4. For the samples T1 and T4 an unimodal distribution is observed with a standard deviation of about 44%. The samples T2 and T3 have a bimodal distribution.

The most known systems, where the bimodal QD size distribution was observed, are SK InAs/GaAs(001) QDs3235, where the bimodal behavior was described in terms of InAs coverage33,34, which is the distinct threshold for the SK dot formation, and SK Ge/Si(001) islands36,37, for whom the morphological shape transition of Ge islands is responsible for the bimodal distribution.

In order to study the origin of the bimodal size distribution in our samples, we investigated the degree of order of the droplet spatial arrangement which can be determined via the Hopkins-Skellam index (IHS) of the droplet ensemble38,39. IHS permits a precise measurement of a spatial regularity of the droplet distribution through the comparison with a purely random spatial distribution of the ensemble elements. IHS is defined as

IHS=i=1Nr1i2i=1Nr2i2, 4

where N is the total number of droplets. The term r1i2 represents the distance to the nearest droplet from a random location in the studied area. Similarly, r2i2 denotes the distance to the nearest droplet from the i-th droplet. Therefore, for a completely random distribution (Poisson) of droplets, IHS = 1. A droplet pattern which shows a clusterization returns a value IHS > 1. The minimum value of IHS is obtained for a perfectly ordered pattern of droplets, such as the hexagonal lattice, which gives IHS = 0.14. Therefore, for the patterns with an intermediate regularity, the value of IHS is expected to be framed between 0.14 to 1, with the IHS value increasing with the disorder.

The dependence of IHS on the deposition temperature is reported in Fig. 6. At low temperatures, the droplets, although randomly located, show a high degree of order, with IHS = 0.35, thus closer to a regular lattice than to a random ensemble. As the temperature reaches the onset of the bimodal distribution (T = 350C), the Hopkins-Skellam index steeply increases to IHS0.5. A marked dependence on the position on the sample is also observed. The droplet distribution regains a partial order only at T=450C, where IHS=0.43±0.01. Thus, the presence of the bimodal distribution of size walks together with a sizeable decrease of a droplet spatial order, which depends on the location on the sample surface.

Figure 6.

Figure 6

The dependence of the Hopkins–Skellam index (IHS) on the deposition temperature.

As already mentioned, we do not observe ripening processes of Ga droplets. Therefore, the bimodal behavior at the intermediate temperature should stems from a different process able to produce multimodal and broad island size distribution. Together with the Hopkins-Skellam analysis of the spatial arrangement of the droplets, this calls for the presence of a temperature activated extrinsic nucleation process, sensible to the local environment, and affecting the growth kinetics of the droplets in the 350–400C temperature range only.

A highly flat and smooth surface was obtained using rather low growth rate and high V/III ratio following the prescription of Ref.16. This prevents the formation of large (with μm lateral dimensions) triangular pyramidal hillocks consisting of up to several tens of steps, nucleated by the staking faults40. The surface morphology of our samples before the droplet deposition is presented on Fig. 7. The surface is very smooth with a root-mean-square (RMS) roughness of only 0.14 nm. Nevertheless, small hillocks consisting of few steps are still present (see e.g. Fig. 8a, where the stepped triangular pyramid with 4–5 steps is observable inside the area highlighted with the blue lines). The hillocks, thus, introduce a sizeable density of steps on an otherwise nearly free singular GaAs(111)A surface.

Figure 7.

Figure 7

10×10μm2 AFM tapping amplitude image of GaAs buffer layer morphology, grown according to Ref.16 and used in this work.

Figure 8.

Figure 8

(a) 1×1μm2 AFM tapping amplitude image of the sample T2. The white lines indicate where the height profiles of islands were measured. The blue lines indicate the area of the stepped hillock. (b) The height profiles of 5 islands of the sample taken from (a).

We then analyzed the local surface morphology for different island size in the sample T2 (see Fig. 8a). The height profiles of five randomly chosen islands are presented in Fig. 8b. The maximum height of islands I1–I3 (which belong to the large droplet mode) is about 9–12 nm. On the contrary the maximum height of the small islands I4–I5 is only 5–6 nm. Taking also into account the slight change in island radius, the big islands show a volume which is roughly four times larger than the one of the small islands. By analyzing the local environment of the islands, we found that the islands originated from the small droplets which are nucleated within flat terrace areas. On the contrary, the large islands from the large droplets are always nucleated at the step edges joining two terraces. It was shown that the surface step is a preferred nucleation site for In droplet formation on GaAs(001)41.

The original surface morphology affects on the droplet size distribution and thus, in turn the island size. A change in the local island density is also observed. The two observations are strictly linked, as an increase in size requires a larger CZ and thus a smaller density. Such local variations of the density, which are restricted to the hillock areas, introduce an additional source of noise in the determination of the ensemble parameters like the nucleation activation energy Ea and the critical cluster size i. However, this effect appears to be small as it does not hinder the correct determination of the two parameters.

Combining the local dependence of the island size and density with the finite temperature range where the bimodal distribution is observed, we can interpret the relationship between the local environment and the droplet size as stemming from the combined effect of the initial droplet nucleation site and the influence of the presence of ES barrier at the step edges on the adatom diffusion length16,21,42.

As a matter of fact, the droplets grow by capturing adatoms roughly within a diffusion length distance from the droplet itself. At low temperature the adatom diffusion length D is small, compared to the average terrace width WT. So, the presence of the ES barrier, which limits the adatom diffusion perpendicularly to the steps, is not affecting the adatom capture kinetics. The actual environment of the nucleation site is not playing a fundamental role at low T, and a unimodal behavior is predicted. As the temperature increases, the diffusion length increases until D>WT. However, the presence of a sizable ES barrier limits the adatom CZ of each droplet within the terrace where the droplet is located. This introduces a broadening effect in the island size which has a marked local dependence, as it depends on the actual terrace width on which the droplet nucleated. In particular, the origin of the bimodal distribution of height is related to the observation that the droplets, nucleated at terrace edges, can collect adatoms from the two contiguous terraces. As the temperature further increases, the droplet CZ size is no more affected by the presence of finite width terraces, as the ES barrier at the step edges can be overcome by adatoms. This makes the CZ size independent from the local environment, thus restoring the unimodal size distribution of the island size.

Conclusions

Ga droplet nucleation dynamics on singular GaAs(111)A substrates, that we analyzed through the CZD approach28,29, is characterized by a small critical nucleus size i = 1-2 atoms. This finding supports the recent critical cluster determination by Ohtake et al.22 based on the droplet density dependence on metal flux. It shows that lower reactivity of GaAs(111)A, respect to GaAs(001), permits the stabilization of smaller predicted magic Ga cluster, constituted by just three atoms43. On the contrary, larger i is observed on GaAs(001) substrates43,44. The single activation energy for the droplet density dependence on the temperature (Ea=1.13±0.23eV) is observed in the whole measured range. At low and high temperature the spatial distribution of the droplets on the surface is remarkably regular, with a HS index IHS=0.35, thus approaching that of the hexagonal lattice (IHS=0.14). The average excluded area around each island is highly symmetrical, with a nearly hexagonal shape with the vertices in <21¯1¯> directions. The shape of the excluded zone suggests that <21¯1¯> directions are preferable for Ga adatom diffusion on GaAs(111)A. This observation is in agreement with Ga-vacancy (2×2) surface reconstruction of GaAs(111)A30,31.

At intermediate temperatures (350–400C) we observe the bimodal size distribution of GaAs islands, connected with a sharp increase of the disorder of the island sites, as measured by the HS index. At T=400C,0.45<IHS<0.55, with a marked dependence on the sample site. We attributed such behavior to the influence of local surface morphology which is sampled by the island CZ during its growth. Wide terraces (tens of nm wide) are observed on the singular GaAs(111)A surface and related to the presence of large and flat hillocks generated by the stacking faults16,40,41. The bimodal size distribution is attributed to the presence of the strong ES barrier at the terrace step edges16, which limits Ga adatom diffusion on the terraces, thus inducing strong differences in the CZ size for droplets are nucleated on the terraces or at the terrace step edges. The same effect is responsible of the increase of IHS index and the local variation.

Acknowledgements

This research was funded by the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement # 721394. We thank Tommaso Radaelli, Stefania Riva, and Marta Tonini for the help in the data analysis.

Author contributions

S.S. and A.T. conceived the experiments. A.T., A.F., and S.B. carried out the sample growth and performed AFM measurements. A.T. performed the island nucleation analysis and the CZD analysis. R.T., S.V., and S.T. performed the Hopkins–Skellam analysis. All authors discussed the results and wrote the manuscript.

Data availability

The datasets generated during and/or analysed during the current study are available from the corresponding author on reasonable request.

Competing interests

The authors declare no competing interests.

Footnotes

Publisher's note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Availability Statement

The datasets generated during and/or analysed during the current study are available from the corresponding author on reasonable request.


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